Earth's Crust in Motion



Vocabulary
Earthquake- the shaking and trembling that results from the movement of rock beneath Earth's surface.
Stress- a force that acts on rock to change its shape or volume.
Shearing- stress that pushes a mass of rock in two opposite directions.
Tension- a force that stretches rock to make it thinner.
Compression- a force that squeezes rocks until it folds or breaks.
Deformation- any change in the volume or shape of Earth's crust.
Fault- a break in Earth's crust where slabs or crust slip past each other.
Strike-slip Faults- a fault where rocks slip past each other sideways with little up-or-down motion.
Normal Faults- a fault that has a hanging wall and footwall that slides downwards.
Reverse faults- the exact opposite of a normal fault, which has a footwall and a hanging wall except sliding upwards.
Friction- the force that opposes the motion of one surface as it moves across another surface.
Fault-block Mountain- normal faults uplifting a block of rock.
folds- bends in rock that form when compression shortens and thickens part of Earth's crust.
Anticline- the fold in rock that bends upward into an arch.
Syncline- a fold in rock that bends downward in the middle to form a bowl.
Plateau- a large area of flat land elevated high above sea level.

Outline


Stress in the Crust

  • Stress
    • the force that changes the shape and volume of rock
      • adds energy to rock

Types of Stress

  • shearing
    • slip and breaks rock
***
* tension
    • pulls on crust
      • stretches rock, so it becomes thinner in the middle
  • compression
    • squeezes rock till folds or breaks
      • like a giant trash compactor
  • deformation
    • changes in the earth's crust

Kinds of Faults

  • faults
    • a break in earth's crust
      • faults occur near boundaries

Strike-Slip Fault

  • shearing
    • causes strike-slip fault
  • boundaries form
    • called transform boundary
    • andyany12345.jpg

Normal Faults

  • tension
    • causes normal faults
      • rock slips
      • fault that lies above is hanging wall
      • fault that lies below is footwall

Reverse Faults

  • compression
    • causes reverse faults
      • reverse faults produce part of Appalachian Mountain

Friction Along Faults


  • Friction
    • a force that opposes the motion of one surface as it moves across another surface
  • Faults sometimes jam together because of friction
    • they will jerk free, which produces small earthquakes
      • stress is strong enough to overcome friction force

Mountain Building

  • forces of plates can build up earth's surface

Mountains formed by Faulting

  • Fault block mountain
    • forms when faults uplift a block of rock
      • Sierra Nevada of California is a fault-block mountain
      • Great Basin also has many ranges of fault block mountain
  • two plates move away from each other
    • creates many normal faults

Mountains formed by Folding

  • Folds
    • plate movement causes crust to fold
    • bends in rock that form compression
  • California's northern Coast Range are partly the result of folding

Anticlines and Synclines

  • A fold in rock that bends upward into an arch is Anticline
    • anticline is the Black Hills
    • Black Hill formed about 65 million years ago
  • A fold in rock that bends downwards into an arch is Syncline
    • syncline can be as large as Illinois
    • The Illinois Basin is a syncline that stretches very far

Plateaus

  • plateaus
    • the force that raises mountains
    • a large area of flat land above sea level
    • a lot of plateau lies more than 1500 meters above sea level

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